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Geology.

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Presentation on theme: "Geology."— Presentation transcript:

1 Geology

2 A Layered Earth No physical samples from beneath outermost layer of earth!!!! Clues from: Heat measurements leaking from interior Chemical composition of volcanic gases Chemical composition of volcanic rock Studies of shocks from distant earthquakes Seismic waves

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4 Lithosphere Cool, rigid, ~60 miles thick Asthenosphere Thin, hot flowing ~430 miles thick

5 A New Age In Geology

6 Continental Drift Puzzle like fit of continents
Even better fit of continental shelves Same fossils on 2 coastlines Coal in Antarctica 1912 Wegener - continental drift Original Land Mass - Pangaea

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10 20th Century Additions to Theory:
Earthquakes/volcanoes not random

11 Dating of seafloor = 200 MYO
Continents BYO Seismic studies suggest molten layer Discovery of Mid Atlantic Ridge

12 Sea Floor Spreading If new material is being formed it should be hot
It is The farther away from the ridge the rock should be younger As it cools and shrinks as it moves away from ridge, it should shrink and increase density It does Sediments should be thicker at edges of oceans than in the middle They are

13 As earth’s magnetic poles reverse, there should be stripes of rock with minerals pointing to where north was at the time. There is

14 Plate Tectonics A new name for the 2 old theories - continental drift and seafloor spreading combined Slow!!!!! 2 inches/year in Atlantic 4.8 cubic miles of new seafloor each year

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16 Types of Plate margins 1) Convergent Plates moving together
When both rise - mountains When one subducts another - volcanoes

17 2) Divergent When plates move apart Creates shallow volcanoes
mid Atlantic rift and Iceland great examples of this

18 3) Transform When plates are rubbing side by side
Pressure builds and they can ‘lurch” Causes earthquakes San Andreas fault


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